Petralogy a Treatise On Rocks volume 1
Petralogy a Treatise On Rocks volume 1
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Id.
Most of the kinds enumerated in the former Structure may also be found in this. For the smallest or very minute grained, see granitin.
Small grained white granite, with siderite, from the summit of Mont Blanc.
White quartz, brown or reddish felspar, and black siderite, from the Italian Alps.
The same, from the Isle of Elba.
Grey granite, with garnets, from Bohemia.
The same, from Norway and Scotland.
Grey granite, from Alencon. This is the com- mon granite used at Paris.
Grey granite, with ...nodules of granitin, from the Alps of Dauphiny.
Light grey granite, with red lines composed of garnets, from Namiest in Moravia.
Grey granite, with veins of basaltin, from Nor- way.
Secondary granite, in thin layers, from the cave ofGribon, Isle of Mull.
MODE V. GRANITE.
STRUCTURE III. VEINED.
Saussure has described this rock with such accuracy and precision, and has himself so distin- guished it from gneiss, that it is surprising it should since have been referred to the latter. In gneiss the veins of mica run parallel through the rock, which regularly splits in their direction.
What to read after Petralogy a Treatise On Rocks volume 1?
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To quickly assess the difficulty of the text, read a short excerpt:
Id.
Most of the kinds enumerated in the former Structure may also be found in this. For the smallest or very minute grained, see granitin.
Small grained white granite, with siderite, from the summit of Mont Blanc.
White quartz, brown or reddish felspar, and black siderite, from the Italian Alps.
The same, from the Isle of Elba.
Grey granite, with garnets, from Bohemia.
The same, from Norway and Scotland.
Grey granite, from Alencon. This is the com- mon granite used at Paris.
Grey granite, with ...nodules of granitin, from the Alps of Dauphiny.
Light grey granite, with red lines composed of garnets, from Namiest in Moravia.
Grey granite, with veins of basaltin, from Nor- way.
Secondary granite, in thin layers, from the cave ofGribon, Isle of Mull.
MODE V. GRANITE.
STRUCTURE III. VEINED.
Saussure has described this rock with such accuracy and precision, and has himself so distin- guished it from gneiss, that it is surprising it should since have been referred to the latter. In gneiss the veins of mica run parallel through the rock, which regularly splits in their direction.
What to read after Petralogy a Treatise On Rocks volume 1?
You can find similar books in the "Read Also" column, or choose other free books by Pinkerton John to read onlineMoreLess
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